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Qinghai lake fluctuation and climatic change singce the last glaciation

  • Wang Sumin
  • Wang Yunfei
  • Wu Ruijin
  • Li Jianren
Article

Abstract

Qinghai Lake is located in a hydrologically closed basin at the conjunction of SE and SW monsoons and westerlies. Its frequent lake level fluctuations arising from climatic and monsoonal changes have left a series of geological records since the last glaciation.

The coarse sediments in Core QD1, the sporopollen assemblage representing steppe, the eolian paleo-sanddunes in the east and southeast banks and the fossil glacial topography all indicated frigid and arid climatic conditions and large scale shrinkage of the lake during the last glacial maximum.

Keywords

Lake Level Qaidam Basin Sandy Gravel Back Edge High Lake Level 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

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Copyright information

© Science Press 1991

Authors and Affiliations

  • Wang Sumin
    • 1
  • Wang Yunfei
    • 1
  • Wu Ruijin
    • 1
  • Li Jianren
    • 1
  1. 1.Nanjing Institute of Geography and LimnologyAcademia SinicaNanjingChina

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